A Special Issue Devoted to the Accretionary and Collisional Tectonics of the Altaids and its Metallogeny  

作　　者：XIAO Wenjiao LIU Yongjiang HOU Zengqian LI Shan 

机构地区：[1]Xinjiang Research Center for Mineral Resources,Xinjiang Institute of Ecology and Geography,Chinese Academy of Sciences,Urumqi 830011,China [2]College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,Beijing 100049,China [3]Key Lab of Submarine Geoscience and Prospecting Techniques,MOE,Institute for Advanced Ocean Study,College o f Marine Geosciences,Ocean University of China,Qingdao 266100,China [4]Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China

出　　处：《Acta Geologica Sinica(English Edition)》2019年第5期I0001-I0006,共6页地质学报（英文版）

摘　　要：Altaids:The conception The Altaids is tectonically sandwiched between the Baltica and Siberia cratons to the north and the Tarim and North China cratons to the south(Sengor et al.,1993).This huge orogen has been also called the Altaid collage(Yakubchuk,2004),Central Asian Orogenic Belt(CAOB)(Jahn et al.,2000a),or Central Asian Orogenic System(Briggs et al.,2007).Long before these terms,the Altaids even had been called the Asian Foldbelt,Ural-Mongolian Foldbelt,or Ural-Amurian Foldbelt,mostly by the former Soviet Union scientists(Yakubchuk,2004).

关 键 词：ALTAI belt Asian 

分 类 号：P54[天文地球—构造地质学]